The Height of F-Layer Irregularities in the Arctic Ionosphere

Results and interpretations of oblique incidence soundings of the arctic ionosphere are presented. Anomalous echoes are found to be prevalent in high latitudes in contrast to lower latitudes where 2F groundscatter predominates. One of the echoes seen regularly at College, Alaska has been identified...

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Main Author: Bates, Howard F.
Format: Report
Language:English
Published: Geophysical Institute at the University of Alaska 1959
Subjects:
Online Access:http://hdl.handle.net/11122/3560
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/3560 2023-05-15T14:59:24+02:00 The Height of F-Layer Irregularities in the Arctic Ionosphere Bates, Howard F. 1959-03 http://hdl.handle.net/11122/3560 en_US eng Geophysical Institute at the University of Alaska http://hdl.handle.net/11122/3560 Geophysical Institute Report 1959 ftunivalaska 2023-02-23T21:36:02Z Results and interpretations of oblique incidence soundings of the arctic ionosphere are presented. Anomalous echoes are found to be prevalent in high latitudes in contrast to lower latitudes where 2F groundscatter predominates. One of the echoes seen regularly at College, Alaska has been identified as direct F-layer (IF) backscatter. The observations of the IF echo provide direct evidence of the presence of irregularities in the F-layer between heights of 350 and 600 km. The IF echoes are recorded regularly at night and occasionally during the day in disturbed periods. They appear to be associated with auroral ionization. Simultaneous reception of 2F echoes from the north and the south indicates that at times the reflecting layer is tilted. Tilt-angles in the vicinity of 2 to 3 degrees are found. The 2F echoes from the north usually connect to the extraordinary branch of the vertical incidence trace while the 2F echoes from the south appear to connect to the ordinary branch. The analysis of groundscattered (2F) echoes is extended from a plane to a spherical geometry, and it is shown that a geometrical extension of the plane earth theory is adequate. The observed range-frequency dependence differs only slightly from that predicted by the latter theory. The research reported in this document has been sponsored by the Electronic Research Directorate of the Air Force Cambridge Research Center, Air Research and Development Command. Air Force Research Contract No. AF 19(604)-1859 Yes Report Arctic Alaska University of Alaska: ScholarWorks@UA Arctic
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Results and interpretations of oblique incidence soundings of the arctic ionosphere are presented. Anomalous echoes are found to be prevalent in high latitudes in contrast to lower latitudes where 2F groundscatter predominates. One of the echoes seen regularly at College, Alaska has been identified as direct F-layer (IF) backscatter. The observations of the IF echo provide direct evidence of the presence of irregularities in the F-layer between heights of 350 and 600 km. The IF echoes are recorded regularly at night and occasionally during the day in disturbed periods. They appear to be associated with auroral ionization. Simultaneous reception of 2F echoes from the north and the south indicates that at times the reflecting layer is tilted. Tilt-angles in the vicinity of 2 to 3 degrees are found. The 2F echoes from the north usually connect to the extraordinary branch of the vertical incidence trace while the 2F echoes from the south appear to connect to the ordinary branch. The analysis of groundscattered (2F) echoes is extended from a plane to a spherical geometry, and it is shown that a geometrical extension of the plane earth theory is adequate. The observed range-frequency dependence differs only slightly from that predicted by the latter theory. The research reported in this document has been sponsored by the Electronic Research Directorate of the Air Force Cambridge Research Center, Air Research and Development Command. Air Force Research Contract No. AF 19(604)-1859 Yes
format Report
author Bates, Howard F.
spellingShingle Bates, Howard F.
The Height of F-Layer Irregularities in the Arctic Ionosphere
author_facet Bates, Howard F.
author_sort Bates, Howard F.
title The Height of F-Layer Irregularities in the Arctic Ionosphere
title_short The Height of F-Layer Irregularities in the Arctic Ionosphere
title_full The Height of F-Layer Irregularities in the Arctic Ionosphere
title_fullStr The Height of F-Layer Irregularities in the Arctic Ionosphere
title_full_unstemmed The Height of F-Layer Irregularities in the Arctic Ionosphere
title_sort height of f-layer irregularities in the arctic ionosphere
publisher Geophysical Institute at the University of Alaska
publishDate 1959
url http://hdl.handle.net/11122/3560
geographic Arctic
geographic_facet Arctic
genre Arctic
Alaska
genre_facet Arctic
Alaska
op_source Geophysical Institute
op_relation http://hdl.handle.net/11122/3560
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